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Saharan dust nutrients promote Vibrio bloom formation in marine surface waters

机译:撒哈拉粉尘养分促进海洋表层水弧菌绽放形成

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摘要

Vibrio is a ubiquitous genus of marine bacteria, typically comprising a small fraction of the total microbial community in surface waters, but capable of becoming a dominant taxon in response to poorly characterized factors. Iron (Fe), often restricted by limited bioavailability and low external supply, is an essential micronutrient that can limit Vibrio growth. Vibrio species have robust metabolic capabilities and an array of Fe-acquisition mechanisms, and are able to respond rapidly to nutrient influx, yet Vibrio response to environmental pulses of Fe remains uncharacterized. Here we examined the population growth of Vibrio after natural and simulated pulses of atmospherically transported Saharan dust, an important and episodic source of Fe to tropical marine waters. As a model for opportunistic bacterial heterotrophs, we demonstrated that Vibrio proliferate in response to a broad range of dust-Fe additions at rapid timescales. Within 24 h of exposure, strains of Vibrio cholerae and Vibrio alginolyticus were able to directly use Saharan dust–Fe to support rapid growth. These findings were also confirmed with in situ field studies; arrival of Saharan dust in the Caribbean and subtropical Atlantic coincided with high levels of dissolved Fe, followed by up to a 30-fold increase of culturable Vibrio over background levels within 24 h. The relative abundance of Vibrio increased from ∼1 to ∼20% of the total microbial community. This study, to our knowledge, is the first to describe Vibrio response to Saharan dust nutrients, having implications at the intersection of marine ecology, Fe biogeochemistry, and both human and environmental health.
机译:弧菌是普遍存在的海洋细菌属,通常占地表水总微生物群落的一小部分,但能够响应特征不明确的因素而成为主要的分类单元。铁(Fe)通常受到生物利用度有限和外部供应不足的限制,是一种必需的微量营养素,会限制弧菌的生长。弧菌具有强大的代谢能力和一系列的Fe捕获机制,并且能够对养分涌入做出快速响应,但对Fe的环境脉冲的弧菌响应仍然没有特征。在这里,我们检查了自然和模拟脉冲传播的大气中撒哈拉尘埃之后的弧菌种群增长情况,撒哈拉尘埃是向热带海洋水域中重要的Fe来源。作为机会细菌异养菌的模型,我们证明了弧菌会在快速的时间尺度响应多种尘埃铁的添加而增殖。在暴露的24小时内,霍乱弧菌和溶藻弧菌菌株能够直接使用撒哈拉粉尘-铁来支持快速生长。这些发现也得到了现场研究的证实。撒哈拉尘埃到达加勒比海和亚热带大西洋的同时,铁的溶解水平很高,随后可培养弧菌在24小时内比背景水平高出30倍。弧菌的相对丰度从总微生物群落的约1%增至约20%。据我们所知,该研究是第一个描述弧菌对撒哈拉尘土养分的反应的研究,对海洋生态学,铁生物地球化学以及人类和环境健康的交叉影响具有重要意义。

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